Near-surface ocean temperature
Near-surface ocean temperature
Date
2006-02-11
Authors
Ward, Brian
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DOI
10.1029/2004JC002689
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Keywords
Air-sea heat flux
Cool skin
Warm layer
Cool skin
Warm layer
Abstract
The first open ocean deployment of the Skin Depth Experimental
Profiler (SkinDeEP) was from the R/V Melville in the Gulf of California during
the Marine Optical Characterization Experiment (MOCE–5). SkinDeEP is
an autonomous, vertical profiler for the upper few meters of the ocean. During
MOCE–5, SkinDeEP was deployed on 10 separate occasions, and profiles were
made at intervals of approximately one minute each. A total of 976 profiles were
acquired during the cruise. The ocean skin temperatures were measured by the
Marine Atmosphere Emitted Radiance Interferometer (M–AERI), an infrared spectroradiometer.
Typical meteorological conditions were of low winds and high
insolation. The dataset provided captures the near-surface temperature structure
that decouples the skin layer from the conventional in–situ bulk sea surface temperature
measurements made at a depth of a few meters. Data from SkinDeEP
showed strong diurnal warming within the upper few meters, with one extreme
case of 4.6 K. There were large discrepancies when computing the skin–bulk
temperature difference with bulk temperatures at different depths. Results also
show the strong dependency of estimating air–sea heat flux based on SST, with
warm–layer errors of almost 60 Wm-2 associated with intense stratification. This
indicates the importance of the inclusion of the skin temperature for accurate
calculation of latent, sensible, and net longwave heat fluxes.
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Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution.
The definitive version was published in Journal of Geophysical Research 111 (2006): C02004, doi:10.1029/2004JC002689.
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Journal of Geophysical Research 111 (2006): C02004